Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum

The maximum glacier extent during the "Little Ice Age" (mid 18th century AD) in Jotunheimen, southern Norway, was mapped using remote sensing techniques. Interpretation of existing glaciochronological studies, analysis of geomorphological maps, and own GPS-field measurements were applied f...

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Published in:The Cryosphere
Main Authors: Baumann, S., Winkler, S., Andreassen, L. M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-3-231-2009
https://tc.copernicus.org/articles/3/231/2009/
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spelling ftcopernicus:oai:publications.copernicus.org:tc1220 2023-05-15T16:21:54+02:00 Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum Baumann, S. Winkler, S. Andreassen, L. M. 2018-09-27 application/pdf https://doi.org/10.5194/tc-3-231-2009 https://tc.copernicus.org/articles/3/231/2009/ eng eng doi:10.5194/tc-3-231-2009 https://tc.copernicus.org/articles/3/231/2009/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-3-231-2009 2020-07-20T16:26:31Z The maximum glacier extent during the "Little Ice Age" (mid 18th century AD) in Jotunheimen, southern Norway, was mapped using remote sensing techniques. Interpretation of existing glaciochronological studies, analysis of geomorphological maps, and own GPS-field measurements were applied for validation of the mapping. The length of glacier centrelines and other inventory data were determined using a Geographical Information System (GIS) and a Digital Elevation Model. "Little Ice Age" maximum extent for a total of 233 glaciers comprising an overall glacier area of about 290 km 2 was mapped. Mean length of the centreline was calculated to 1.6 km. Until AD 2003, the area and length shrank by 35% and 34%, respectively, compared with the maximum "Little Ice Age" extent. Text glacier Copernicus Publications: E-Journals Norway The Cryosphere 3 2 231 243
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The maximum glacier extent during the "Little Ice Age" (mid 18th century AD) in Jotunheimen, southern Norway, was mapped using remote sensing techniques. Interpretation of existing glaciochronological studies, analysis of geomorphological maps, and own GPS-field measurements were applied for validation of the mapping. The length of glacier centrelines and other inventory data were determined using a Geographical Information System (GIS) and a Digital Elevation Model. "Little Ice Age" maximum extent for a total of 233 glaciers comprising an overall glacier area of about 290 km 2 was mapped. Mean length of the centreline was calculated to 1.6 km. Until AD 2003, the area and length shrank by 35% and 34%, respectively, compared with the maximum "Little Ice Age" extent.
format Text
author Baumann, S.
Winkler, S.
Andreassen, L. M.
spellingShingle Baumann, S.
Winkler, S.
Andreassen, L. M.
Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum
author_facet Baumann, S.
Winkler, S.
Andreassen, L. M.
author_sort Baumann, S.
title Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum
title_short Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum
title_full Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum
title_fullStr Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum
title_full_unstemmed Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum
title_sort mapping glaciers in jotunheimen, south-norway, during the "little ice age" maximum
publishDate 2018
url https://doi.org/10.5194/tc-3-231-2009
https://tc.copernicus.org/articles/3/231/2009/
geographic Norway
geographic_facet Norway
genre glacier
genre_facet glacier
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-3-231-2009
https://tc.copernicus.org/articles/3/231/2009/
op_doi https://doi.org/10.5194/tc-3-231-2009
container_title The Cryosphere
container_volume 3
container_issue 2
container_start_page 231
op_container_end_page 243
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